Micro-Raman and micro-infrared spectra of the silicate and OH-stretchi
ng regions have been obtained from a well-characterized crystal of hyd
rous beta-Mg2SiO4 containing approximately 2.6 wt.% H2O. Five distinct
OH-stretching vibrations were observed in two separate spectral group
ings. A Raman-active band at 3355 cm(-1) and an infrared band at 3351
cm(-1) comprise the first group; a Raman band at 3583 cm(-1) and infra
red bands at 3596 and 3653 cm(-1) make up the second group. These resu
lts are consistent with the incorporation of H into the O1 site. The a
pparent division of the OH-stretching bands into a group near 3330 cm(
-1) and a group near 3600 cm(-1) is due to differences in the lengths
of the hydrogen bonds to the nearest-neighbor oxygen atoms in the Mg2
and Mg3 octahedra. Relative intensities of the bands suggest that a ma
jority of shorter, and hence, stronger hydrogen bonds are formed in th
e hydrated beta phase. Tentative assignments of the observed bands hav
e been made by comparison with the corresponding spectra of anhydrous
beta-Mg2SiO4.